On the Upper Limit of Thermal Inversion During a Misty Sunset Over the Gulf of Trieste, with Advection Fog in the Lower Air Layers; Trieste City Karst Ridge "Srednji Vršič" Top (445m a.s.l.), FVG, Italia
23-February-2021: the African anticyclone, with very mild and dry air at medium/high altitude and adiabatic pressure towards the ground, causes the stagnation of humid air on the relatively cold Gulf of Trieste (in winter-early spring, due to shallow water and many fresh water sources).
It is dense air, saturated with water vapor that condenses on the surface of the sea and then moves towards the surrounding coasts in the form of maritime advection fog with lower temperatures on the sea than in the interior.
On the Upper Limit of Thermal Inversion During a Misty Sunset Over the Gulf of Trieste, with Advection Fog in the Lower Air Layers; Trieste City Karst Ridge "Srednji Vršič" Top (445m a.s.l.), FVG, Italia
23-February-2021: the African anticyclone, with very mild and dry air at medium/high altitude and adiabatic pressure towards the ground, causes the stagnation of humid air on the relatively cold Gulf of Trieste (in winter-early spring, due to shallow water and many fresh water sources).
It is dense air, saturated with water vapor that condenses on the surface of the sea and then moves towards the surrounding coasts in the form of maritime advection fog with lower temperatures on the sea than in the interior.